Zobrazeno 1 - 6
of 6
pro vyhledávání: '"T. N. Shishakova"'
Publikováno v:
Bulletin of the Academy of Sciences, USSR Division of Chemical Science. 14:1086-1088
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::afcf88c8de5f930385c6dd6323569898
https://doi.org/10.1007/bf00845773
https://doi.org/10.1007/bf00845773
Autor:
T. N. Shishakova, M. M. Dubinin
Publikováno v:
Bulletin of the Academy of Sciences, USSR Division of Chemical Science. 15:1954-1956
1. A noticeable decrease in the parameter of the crystal unit cell, representing 2.6%, is observed as the result of the limiting adsorption of water on dehydrated hydro sodalite. 2. A more than one order of magnitude smaller and opposite change in th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fcefa26b3dc49cdd9717a48097f38453
https://doi.org/10.1007/bf01179712
https://doi.org/10.1007/bf01179712
Publikováno v:
Chemistry and Technology of Fuels and Oils. 1:787-789
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f89e83d58b259134c806a07ce03e94a2
https://doi.org/10.1007/bf00718684
https://doi.org/10.1007/bf00718684
Autor:
T. N. Shishakova, É. É. Senderov
Publikováno v:
Bulletin of the Academy of Sciences of the USSR Division of Chemical Science. 16:151-153
1. In the crystallization of sodium zeolites of the chabazite-gmelinite group, the introduction of a high amount of silica into the structure favors the linkage of the hexagonal prisms in the manner characteristic for gmelinite and leads to the forma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3ec1042f68f07a6623fa1c6e04a51298
https://doi.org/10.1007/bf00907118
https://doi.org/10.1007/bf00907118
Autor:
G. M. Fedorova, T. N. Shishakova
Publikováno v:
Bulletin of the Academy of Sciences of the USSR Division of Chemical Science. 16:1782-1784
1. The mineral gmelinite which has been studied belongs to the hexagonal syngony. 2. The parameter of the elementary cell has been doubled along the C axis.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ced2a84abd8a61add227ce3a6a9ef59d
https://doi.org/10.1007/bf00906837
https://doi.org/10.1007/bf00906837
Autor:
T. N. Shishakova, M. M. Dubinin
Publikováno v:
Bulletin of the Academy of Sciences, USSR Division of Chemical Science. 14:1277-1279
The sodium ions in zeolite G are not located in the openings of the six-membered oxygen windows, but are shifted toward the center of the cubic octahedral cavities.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5f3904170ff05859c9baa364521f2501
https://doi.org/10.1007/bf00847922
https://doi.org/10.1007/bf00847922